Feldspars from pegmatites of Ravne in Carinthia
AbstractFeldspars of the Ravne pegmatites are composed of microcline, transitional varieties from orthoclase to microcline, and plagioclases showing characteristics from albite to oligoclase having 9 ½ percent anorthite on the average. The origin of the Ravne pegmatites is explained by the mobilization during a regional metamorphism. Their age is admitted to be Variscan.
How to Cite
Faninger, E. (1981). Feldspars from pegmatites of Ravne in Carinthia. Geologija, 24(1), 75–87. Retrieved from https://www.geologija-revija.si/index.php/geologija/article/view/485